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How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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The Royal Society Publishing
2012
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3261436/ https://www.ncbi.nlm.nih.gov/pubmed/22291221 http://dx.doi.org/10.1098/rsta.2011.0316 |
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author | Kleidon, Axel |
author_facet | Kleidon, Axel |
author_sort | Kleidon, Axel |
collection | PubMed |
description | The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining disequilibrium in a thermodynamic variable requires the extraction of power from another thermodynamic gradient, and the second law of thermodynamics imposes fundamental limits on how much power can be extracted. With this approach and associated limits, I show that the ability of abiotic processes to generate geochemical free energy that can be used to transform the surface–atmosphere environment is strongly limited to less than 1 TW. Photosynthetic life generates more than 200 TW by performing photochemistry, thereby substantiating the notion that a geochemical composition far from equilibrium can be a sign for strong biotic activity. Present-day free energy consumption by human activity in the form of industrial activity and human appropriated net primary productivity is of the order of 50 TW and therefore constitutes a considerable term in the free energy budget of the planet. When aiming to predict the future of the planet, we first note that since global changes are closely related to this consumption of free energy, and the demands for free energy by human activity are anticipated to increase substantially in the future, the central question in the context of predicting future global change is then how human free energy demands can increase sustainably without negatively impacting the ability of the Earth system to generate free energy. This question could be evaluated with climate models, and the potential deficiencies in these models to adequately represent the thermodynamics of the Earth system are discussed. Then, I illustrate the implications of this thermodynamic perspective by discussing the forms of renewable energy and planetary engineering that would enhance the overall free energy generation and, thereby ‘empower’ the future of the planet. |
format | Online Article Text |
id | pubmed-3261436 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2012 |
publisher | The Royal Society Publishing |
record_format | MEDLINE/PubMed |
spelling | pubmed-32614362012-03-13 How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? Kleidon, Axel Philos Trans A Math Phys Eng Sci Articles The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining disequilibrium in a thermodynamic variable requires the extraction of power from another thermodynamic gradient, and the second law of thermodynamics imposes fundamental limits on how much power can be extracted. With this approach and associated limits, I show that the ability of abiotic processes to generate geochemical free energy that can be used to transform the surface–atmosphere environment is strongly limited to less than 1 TW. Photosynthetic life generates more than 200 TW by performing photochemistry, thereby substantiating the notion that a geochemical composition far from equilibrium can be a sign for strong biotic activity. Present-day free energy consumption by human activity in the form of industrial activity and human appropriated net primary productivity is of the order of 50 TW and therefore constitutes a considerable term in the free energy budget of the planet. When aiming to predict the future of the planet, we first note that since global changes are closely related to this consumption of free energy, and the demands for free energy by human activity are anticipated to increase substantially in the future, the central question in the context of predicting future global change is then how human free energy demands can increase sustainably without negatively impacting the ability of the Earth system to generate free energy. This question could be evaluated with climate models, and the potential deficiencies in these models to adequately represent the thermodynamics of the Earth system are discussed. Then, I illustrate the implications of this thermodynamic perspective by discussing the forms of renewable energy and planetary engineering that would enhance the overall free energy generation and, thereby ‘empower’ the future of the planet. The Royal Society Publishing 2012-03-13 /pmc/articles/PMC3261436/ /pubmed/22291221 http://dx.doi.org/10.1098/rsta.2011.0316 Text en This journal is © 2012 The Royal Society http://creativecommons.org/licenses/by/3.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
spellingShingle | Articles Kleidon, Axel How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title | How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title_full | How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title_fullStr | How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title_full_unstemmed | How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title_short | How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
title_sort | how does the earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? |
topic | Articles |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3261436/ https://www.ncbi.nlm.nih.gov/pubmed/22291221 http://dx.doi.org/10.1098/rsta.2011.0316 |
work_keys_str_mv | AT kleidonaxel howdoestheearthsystemgenerateandmaintainthermodynamicdisequilibriumandwhatdoesitimplyforthefutureoftheplanet |